https://www.coastalwiki.org/w/index.php?title=Coastal_Erosion_along_the_Changjiang_Deltaic_Shoreline&feed=atom&action=history
Coastal Erosion along the Changjiang Deltaic Shoreline - Revision history
2024-03-29T11:25:30Z
Revision history for this page on the wiki
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https://www.coastalwiki.org/w/index.php?title=Coastal_Erosion_along_the_Changjiang_Deltaic_Shoreline&diff=78557&oldid=prev
Dronkers J at 15:56, 2 January 2021
2021-01-02T15:56:58Z
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<td colspan="2" style="background-color: #fff; color: #222; text-align: center;">Revision as of 15:56, 2 January 2021</td>
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<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* [[Accretion and erosion for different coastal types]]</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* [[Accretion and erosion for different coastal types]]</div></td></tr>
<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del class="diffchange diffchange-inline">* [[Estuaries and tidal rivers]]</del></div></td><td class='diff-marker'>+</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div> </div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==References==</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==References==</div></td></tr>
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Dronkers J
https://www.coastalwiki.org/w/index.php?title=Coastal_Erosion_along_the_Changjiang_Deltaic_Shoreline&diff=77853&oldid=prev
Dronkers J at 18:50, 2 September 2020
2020-09-02T18:50:05Z
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<td colspan="2" style="background-color: #fff; color: #222; text-align: center;">Revision as of 18:50, 2 September 2020</td>
</tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l10" >Line 10:</td>
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<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Since the early 1980s, the sediment supply to the coastal system in North China has been reduced dramatically because of the extensive hydroengineering works. For example, after the construction of the water diversion scheme which transfers water from the Luanhe River to the Tianjin and Tangshan areas, the annual sediment discharge into the Bohai Sea decreased rapidly from 22·19 to 1·03 million ton/y. Such a decrease in sediment supply has resulted in a maximum [[coastline retreat|coastal retreat]] of 300 m year"1 in the Luanhe River mouth and an average erosion of 25m/y in its offshore sandbars, accompanied by a rapid decrease in sand-bar size.  </div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Since the early 1980s, the sediment supply to the coastal system in North China has been reduced dramatically because of the extensive hydroengineering works. For example, after the construction of the water diversion scheme which transfers water from the Luanhe River to the Tianjin and Tangshan areas, the annual sediment discharge into the Bohai Sea decreased rapidly from 22·19 to 1·03 million ton/y. Such a decrease in sediment supply has resulted in a maximum [[coastline retreat|coastal retreat]] of 300 m year"1 in the Luanhe River mouth and an average erosion of 25m/y in its offshore sandbars, accompanied by a rapid decrease in sand-bar size.  </div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>   </div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>   </div></td></tr>
<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>[[image:figure 1_wang.jpg|thumb|<del class="diffchange diffchange-inline">625px</del>|<del class="diffchange diffchange-inline">left</del>| The geographical setting of the Changjiang River and its catchment basin with locations of the Three-gorge Dam and the south-to-north water diversion schemes]]</div></td><td class='diff-marker'>+</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>[[image:figure 1_wang.jpg|thumb|<ins class="diffchange diffchange-inline">700px</ins>|<ins class="diffchange diffchange-inline">center</ins>| The geographical setting of the Changjiang River and its catchment basin with locations of the Three-gorge Dam and the south-to-north water diversion schemes]]</div></td></tr>
<tr><td colspan="2"> </td><td class='diff-marker'>+</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div> </div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Within the Changjiang River catchment, soil erosion due to cultivation and hill farming has increased over the past decades. However, more and more eroded soil has been trapped by newly constructed reservoirs, and there is no net increase in sediment discharge from the upper catchment of the Changjiang. In fact, a slow decline in sediment supply into the deltaic area has become obvious recently, particularly along the south coast, adjacent to Hangzhou Bay, where [[shoreline]] retreat has been severe.  </div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Within the Changjiang River catchment, soil erosion due to cultivation and hill farming has increased over the past decades. However, more and more eroded soil has been trapped by newly constructed reservoirs, and there is no net increase in sediment discharge from the upper catchment of the Changjiang. In fact, a slow decline in sediment supply into the deltaic area has become obvious recently, particularly along the south coast, adjacent to Hangzhou Bay, where [[shoreline]] retreat has been severe.  </div></td></tr>
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<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td></tr>
<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>[[image:figure 2_wang.jpg|thumb|<del class="diffchange diffchange-inline">550px</del>|<del class="diffchange diffchange-inline">right</del>| Development of the Changjiang River delta and shoreline movements]]</div></td><td class='diff-marker'>+</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>[[image:figure 2_wang.jpg|thumb|<ins class="diffchange diffchange-inline">700px</ins>|<ins class="diffchange diffchange-inline">center</ins>| Development of the Changjiang River delta and shoreline movements]]</div></td></tr>
<tr><td colspan="2"> </td><td class='diff-marker'>+</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div> </div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Future prospects of shoreline movement==  </div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Future prospects of shoreline movement==  </div></td></tr>
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Dronkers J
https://www.coastalwiki.org/w/index.php?title=Coastal_Erosion_along_the_Changjiang_Deltaic_Shoreline&diff=76986&oldid=prev
Dronkers J at 11:04, 5 July 2020
2020-07-05T11:04:02Z
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<td colspan="2" style="background-color: #fff; color: #222; text-align: center;">Revision as of 11:04, 5 July 2020</td>
</tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l49" >Line 49:</td>
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<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* [[Classification of sandy coastlines]]</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* [[Classification of sandy coastlines]]</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* [[Coast erosion]]</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* [[Coast erosion]]</div></td></tr>
<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>* [[<del class="diffchange diffchange-inline">Types and background of </del>coastal erosion]]</div></td><td class='diff-marker'>+</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>* [[<ins class="diffchange diffchange-inline">Dealing with </ins>coastal erosion]]</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* [[Human causes of coastal erosion]]</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* [[Human causes of coastal erosion]]</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* [[Accretion and erosion for different coastal types]]</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* [[Accretion and erosion for different coastal types]]</div></td></tr>
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Dronkers J
https://www.coastalwiki.org/w/index.php?title=Coastal_Erosion_along_the_Changjiang_Deltaic_Shoreline&diff=76876&oldid=prev
Dronkers J at 14:28, 30 June 2020
2020-06-30T14:28:46Z
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<td colspan="2" style="background-color: #fff; color: #222; text-align: center;">Revision as of 14:28, 30 June 2020</td>
</tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l46" >Line 46:</td>
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<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>The overall trend for the next few decades will be the stagnation of sedimentation within the Changjiang estuary, and some sections of the shoreline will be under erosion. Such a significant deficiency in sediment supply, together with the anticipated rise of relative sea-level, will pose a great problem to the potential coastal land resource and coastal protection. As a result, the availability of intertidal land for reclamation will be significantly reduced. Consequently, to sustain agricultural production, particularly peri-urban agricultural, will become a big challenge to the local communities. Furthermore, the coastal [[ecosystems]] will be under threat. It is necessary to further investigate the sediment budget within the estuarine system</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>The overall trend for the next few decades will be the stagnation of sedimentation within the Changjiang estuary, and some sections of the shoreline will be under erosion. Such a significant deficiency in sediment supply, together with the anticipated rise of relative sea-level, will pose a great problem to the potential coastal land resource and coastal protection. As a result, the availability of intertidal land for reclamation will be significantly reduced. Consequently, to sustain agricultural production, particularly peri-urban agricultural, will become a big challenge to the local communities. Furthermore, the coastal [[ecosystems]] will be under threat. It is necessary to further investigate the sediment budget within the estuarine system</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td></tr>
<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>==<del class="diffchange diffchange-inline">See also</del>==</div></td><td class='diff-marker'>+</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>==<ins class="diffchange diffchange-inline">Related articles</ins>==</div></td></tr>
<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div> </div></td><td colspan="2"> </td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* [[Classification of sandy coastlines]]</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* [[Classification of sandy coastlines]]</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* [[Coast erosion]]</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* [[Coast erosion]]</div></td></tr>
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Dronkers J
https://www.coastalwiki.org/w/index.php?title=Coastal_Erosion_along_the_Changjiang_Deltaic_Shoreline&diff=76472&oldid=prev
Dronkers J at 16:17, 29 February 2020
2020-02-29T16:17:18Z
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<td colspan="2" style="background-color: #fff; color: #222; text-align: center;">Revision as of 16:17, 29 February 2020</td>
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<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td></tr>
<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>* [[Classification of coastlines]]</div></td><td class='diff-marker'>+</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>* [[Classification of <ins class="diffchange diffchange-inline">sandy </ins>coastlines]]</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* [[Coast erosion]]</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* [[Coast erosion]]</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* [[Types and background of coastal erosion]]</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* [[Types and background of coastal erosion]]</div></td></tr>
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Dronkers J
https://www.coastalwiki.org/w/index.php?title=Coastal_Erosion_along_the_Changjiang_Deltaic_Shoreline&diff=74791&oldid=prev
Dronkers J at 10:47, 28 June 2019
2019-06-28T10:47:02Z
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<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|AuthorFullName=Quing Wang}}</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|AuthorFullName=Quing Wang}}</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td></tr>
<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div> </div></td><td class='diff-marker'>+</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>[[Category:Coastal <ins class="diffchange diffchange-inline">protection</ins>]]</div></td></tr>
<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>[[Category:Coastal <del class="diffchange diffchange-inline">and marine human activities</del>]]</div></td><td class='diff-marker'>+</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>[[Category:<ins class="diffchange diffchange-inline">Physical coastal and marine processes</ins>]]</div></td></tr>
<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>[[Category:<del class="diffchange diffchange-inline">East Asian Seas</del>]]</div></td><td colspan="2"> </td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>[[Category:Estuaries and tidal rivers]]</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>[[Category:Estuaries and tidal rivers]]</div></td></tr>
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<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;">[[Category:Case studies]]</del></div></td><td colspan="2"> </td></tr>
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Dronkers J
https://www.coastalwiki.org/w/index.php?title=Coastal_Erosion_along_the_Changjiang_Deltaic_Shoreline&diff=73546&oldid=prev
Dronkers J at 12:04, 23 September 2018
2018-09-23T12:04:18Z
<p></p>
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<td colspan="2" style="background-color: #fff; color: #222; text-align: center;">Revision as of 12:04, 23 September 2018</td>
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<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Future prospects of shoreline movement==  </div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Future prospects of shoreline movement==  </div></td></tr>
<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>Previous studies indicate that the changes in sediment input into the coastal system are dependent on the two factors: (1) the [[sediment]] output from the Changjiang River basin to the estuary; and (2) from the river [[estuary]] to the south coast system. The sediment output from the drainage basin is determined by the sediment source available and the hydrological processes, on which human activities have exerted more and more effects. The sediments are redistributed by currents through the four tidal channels after they enter into the estuary. The [[sediment transport]] direction altered as the principal sediment transport route shifts its way from one channel to another.The shorelines along main waterways and along the south coast around Jinshan are very sensitive to the changes in the suspended sediment supply from the Changjiang River. It is anticipated that the sediment supply will decrease significantly due to the following engineering projects.  </div></td><td class='diff-marker'>+</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>Previous studies indicate that the changes in sediment input into the coastal system are dependent on the two factors: (1) the [[sediment]] output from the Changjiang River basin to the estuary; and (2) from the river [[estuary]] to the south coast system. The sediment output from the drainage basin is determined by the sediment source available and the hydrological processes, on which human activities have exerted more and more effects. The sediments are redistributed by currents through the four tidal channels after they enter into the estuary. The [[<ins class="diffchange diffchange-inline">Definitions of coastal terms|</ins>sediment transport]] direction altered as the principal sediment transport route shifts its way from one channel to another.The shorelines along main waterways and along the south coast around Jinshan are very sensitive to the changes in the suspended sediment supply from the Changjiang River. It is anticipated that the sediment supply will decrease significantly due to the following engineering projects.  </div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===The Three-gorge Dam as a sediment trap===</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===The Three-gorge Dam as a sediment trap===</div></td></tr>
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Dronkers J
https://www.coastalwiki.org/w/index.php?title=Coastal_Erosion_along_the_Changjiang_Deltaic_Shoreline&diff=35398&oldid=prev
Cliviahaese: /* References */
2009-11-04T09:07:09Z
<p><span dir="auto"><span class="autocomment">References</span></span></p>
<table class="diff diff-contentalign-left" data-mw="interface">
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<td colspan="2" style="background-color: #fff; color: #222; text-align: center;">Revision as of 09:07, 4 November 2009</td>
</tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l59" >Line 59:</td>
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<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Chen, X., 1996. An integrated study of sediment discharge from the Changjiang River, China, and the delta development since the mid-Holocene, J. Coastal Res. 12(1): 26-37.</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Chen, X., 1996. An integrated study of sediment discharge from the Changjiang River, China, and the delta development since the mid-Holocene, J. Coastal Res. 12(1): 26-37.</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td></tr>
<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>Chen, X. & Chen, J. 1997. Effect of the south-to-north water diversion on the coarse-grained sediment discharge into the Yangtz River Estuary, Advances in Water Science 8 (3), pp. 259–263 (in Chinese with an English abstract). <del class="diffchange diffchange-inline">doi:10.1016/S0038-1098(97)80030-0</del></div></td><td class='diff-marker'>+</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>Chen, X. & Chen, J. 1997. Effect of the south-to-north water diversion on the coarse-grained sediment discharge into the Yangtz River Estuary, Advances in Water Science 8 (3), pp. 259–263 (in Chinese with an English abstract).  </div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Higgitt, D.L. & Lu, X.X., 1996. Patterns of sediment yield in the Upper Yangtze Basin, China. In: Walling, D.E. and Webb, B.W. (ed.), 1996. Erosion and Sediment Yield: Global and Regional Perspectives. IAHS Publ. no. 236, pp. 205–214.</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Higgitt, D.L. & Lu, X.X., 1996. Patterns of sediment yield in the Upper Yangtze Basin, China. In: Walling, D.E. and Webb, B.W. (ed.), 1996. Erosion and Sediment Yield: Global and Regional Perspectives. IAHS Publ. no. 236, pp. 205–214.</div></td></tr>
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Cliviahaese
https://www.coastalwiki.org/w/index.php?title=Coastal_Erosion_along_the_Changjiang_Deltaic_Shoreline&diff=35377&oldid=prev
Cliviahaese: /* References */
2009-10-28T14:37:55Z
<p><span dir="auto"><span class="autocomment">References</span></span></p>
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<td colspan="2" style="background-color: #fff; color: #222; text-align: center;">Revision as of 14:37, 28 October 2009</td>
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<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td></tr>
<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>Chen, X., 1996. An integrated study of sediment discharge from the Changjiang River, China, and the delta development since the mid-Holocene, J. Coastal Res. 12: 26.</div></td><td class='diff-marker'>+</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>Chen, X., 1996. An integrated study of sediment discharge from the Changjiang River, China, and the delta development since the mid-Holocene, J. Coastal Res. 12<ins class="diffchange diffchange-inline">(1)</ins>: 26<ins class="diffchange diffchange-inline">-37</ins>.</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Chen, X. & Chen, J. 1997. Effect of the south-to-north water diversion on the coarse-grained sediment discharge into the Yangtz River Estuary, Advances in Water Science 8 (3), pp. 259–263 (in Chinese with an English abstract). doi:10.1016/S0038-1098(97)80030-0</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Chen, X. & Chen, J. 1997. Effect of the south-to-north water diversion on the coarse-grained sediment discharge into the Yangtz River Estuary, Advances in Water Science 8 (3), pp. 259–263 (in Chinese with an English abstract). doi:10.1016/S0038-1098(97)80030-0</div></td></tr>
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Cliviahaese
https://www.coastalwiki.org/w/index.php?title=Coastal_Erosion_along_the_Changjiang_Deltaic_Shoreline&diff=35376&oldid=prev
Cliviahaese: /* References */
2009-10-28T14:26:48Z
<p><span dir="auto"><span class="autocomment">References</span></span></p>
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<td colspan="2" style="background-color: #fff; color: #222; text-align: center;">← Older revision</td>
<td colspan="2" style="background-color: #fff; color: #222; text-align: center;">Revision as of 14:26, 28 October 2009</td>
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<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==References==</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==References==</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td></tr>
<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>Chen, X. <del class="diffchange diffchange-inline">"</del>An integrated study of sediment discharge from the Changjiang River, China, and the delta development<del class="diffchange diffchange-inline">"</del>, <del class="diffchange diffchange-inline">Science in China Series B</del>: <del class="diffchange diffchange-inline">Chemistry, Volume 44, August 2001</del></div></td><td class='diff-marker'>+</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>Chen, X.<ins class="diffchange diffchange-inline">, 1996. </ins>An integrated study of sediment discharge from the Changjiang River, China, and the delta development <ins class="diffchange diffchange-inline">since the mid-Holocene</ins>, <ins class="diffchange diffchange-inline">J. Coastal Res. 12</ins>: <ins class="diffchange diffchange-inline">26.</ins></div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td></tr>
<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>Chen, X. & Chen, J. <del class="diffchange diffchange-inline">Effects </del>of the south-to-north water diversion on the coarse-grained sediment discharge into the <del class="diffchange diffchange-inline">Changjiang </del>Estuary <del class="diffchange diffchange-inline">over the next decades</del>, <del class="diffchange diffchange-inline">Journal of Marine </del>Science, <del class="diffchange diffchange-inline">April 2009</del></div></td><td class='diff-marker'>+</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>Chen, X. & Chen, J. <ins class="diffchange diffchange-inline">1997. Effect </ins>of the south-to-north water diversion on the coarse-grained sediment discharge into the <ins class="diffchange diffchange-inline">Yangtz River </ins>Estuary, <ins class="diffchange diffchange-inline">Advances in Water </ins>Science <ins class="diffchange diffchange-inline">8 (3)</ins>, <ins class="diffchange diffchange-inline">pp. 259–263 (in Chinese with an English abstract). doi:10.1016/S0038-1098(97)80030-0</ins></div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td></tr>
<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>Higgitt, D. L. & Lu, X. Patterns of sediment yield in the Upper Yangtze <del class="diffchange diffchange-inline">basin</del>, China. In Erosion and Sediment Yield: Global and Regional Perspectives<del class="diffchange diffchange-inline">, </del>IAHS Publ. no. 236, <del class="diffchange diffchange-inline">1996</del></div></td><td class='diff-marker'>+</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>Higgitt, D.L. & Lu, X<ins class="diffchange diffchange-inline">.X., 1996</ins>. Patterns of sediment yield in the Upper Yangtze <ins class="diffchange diffchange-inline">Basin</ins>, China. In<ins class="diffchange diffchange-inline">: Walling, D.E. and Webb, B.W. (ed.), 1996. </ins>Erosion and Sediment Yield: Global and Regional Perspectives<ins class="diffchange diffchange-inline">. </ins>IAHS Publ. no. 236, <ins class="diffchange diffchange-inline">pp. 205–214.</ins></div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td></tr>
<tr><td class='diff-marker'>−</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>Lu, X. & Higgitt, D. L. Recent changes of sediment yield in the Upper Yangtze, China</div></td><td class='diff-marker'>+</td><td style="color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>Lu, X. & Higgitt, D. L<ins class="diffchange diffchange-inline">. 1998</ins>. Recent changes of sediment yield in the Upper Yangtze, China<ins class="diffchange diffchange-inline">. Environmental Management 22, 697–709.</ins></div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Xu, H. Impact of the Three-gorge Engineering Works on the deltaic coastal erosion processes. In: Impacts of the Three Gorge Engineering Works on Shanghai and the Counter-measure Study. Research Program Group under the Sciences & Technology Committee, Shanghai Municipal Government, pp. 35–41 (in Chinese)</div></td><td class='diff-marker'> </td><td style="background-color: #f8f9fa; color: #222; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Xu, H. Impact of the Three-gorge Engineering Works on the deltaic coastal erosion processes. In: Impacts of the Three Gorge Engineering Works on Shanghai and the Counter-measure Study. Research Program Group under the Sciences & Technology Committee, Shanghai Municipal Government, pp. 35–41 (in Chinese)</div></td></tr>
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